BELTS OF ARID AND HUMID SEDIMENTATION DURING THE CONIACIAN-MAASTRICHTIAN AGES OF THE LATE CRETACEOUS
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dc.contributor.author | Zharkov M.A. | |
dc.date.accessioned | 2020-12-31T03:46:34Z | |
dc.date.available | 2020-12-31T03:46:34Z | |
dc.date.issued | 1998 | |
dc.identifier | https://elibrary.ru/item.asp?id=13305498 | |
dc.identifier.citation | Stratigraphy and Geological Correlation, 1998, , 5, 429-439 | |
dc.identifier.issn | 0869-5938 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/21882 | |
dc.description.abstract | The existence of six climatic belts - northern circumpolar humid coal, northern mid-latitude coal-bauxite-kaolinite, northern arid tropical-subtropical evaporite, equatorial humid coal-bauxite-kaolinite, southern arid tropical-subtropical evaporite, and southern humid coal-bauxite-kaolinite - are substantiated. Regular secular variations in latitudinal position of arid and humid belts related to global climate warming and general humidization at the end of the Late Cretaceous epoch are outlined. | |
dc.subject | Maastrichtian | en |
dc.subject | Coniacian | en |
dc.subject | Cretaceous | en |
dc.title | BELTS OF ARID AND HUMID SEDIMENTATION DURING THE CONIACIAN-MAASTRICHTIAN AGES OF THE LATE CRETACEOUS | |
dc.type | Статья | |
dc.subject.age | Mesozoic::Cretaceous::Upper::Coniacian | en |
dc.subject.age | Mesozoic::Cretaceous | en |
dc.subject.age | Мезозой::Меловая | ru |
dc.subject.age | Мезозой::Меловая::Верхний::Коньякский | ru |
dc.subject.age | Мезозой::Меловая::Верхний::Маастрихтский | ru |
dc.subject.age | Mesozoic::Cretaceous::Upper::Maastrichtian | en |
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